Articles | Volume 21, issue 11
Hydrol. Earth Syst. Sci., 21, 5875–5889, 2017
https://doi.org/10.5194/hess-21-5875-2017
Hydrol. Earth Syst. Sci., 21, 5875–5889, 2017
https://doi.org/10.5194/hess-21-5875-2017
Research article
27 Nov 2017
Research article | 27 Nov 2017

Impacts of changes in groundwater recharge on the isotopic composition and geochemistry of seasonally ice-covered lakes: insights for sustainable management

Marie Arnoux et al.

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Cited articles

Alexandru, A. and Sushama, L.: Impact of land-use and land-cover changes on CRCM5 climate projections over North America for the twenty-first century, Clim. Dynam., 47, 1197, https://doi.org/10.1007/s00382-015-2896-3, 2016.
Arakawa, A. and Lamb, W. R.: Computational design of the basic dynamical processes of the UCLA general circulation model General circulation models of the atmosphere, Academic Press Inc, New York (A78-10662 01-47), 173–265, 1977.
Arnoux, M., Barbecot, F., Gibert-Brunet, E., Gibson, J., Rosa, E., and Noret, A., and Monvoisin, G.: Geochemical and isotopic mass balances of kettle lakes in southern Quebec (Canada) as tools to document variations in groundwater quantity and quality, Environ. Earth Sci., 76, 106, https://doi.org/10.1007/s12665-017-6410-6, 2017a.
Arnoux, M., Gibert-Brunet, E., Barbecot, F., Gillon, S., Gibson, J., and Noret, A.: Interactions between groundwater and seasonally ice-covered lakes: Using water stable isotopes and radon-222 multilayer mass balance models, Hydrol. Process., 31, 2566–2581, 2017b.
Arora, V. K. and Boer, G. J.: Uncertainties in the 20th century carbon budget associated with land use change, Glob. Change Biol., 16, 3327–3348, https://doi.org/10.1111/j.1365-2486.2010.02202.x, 2010.
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Short summary
Future climate and recharge change scenarios are tested on lake hydrological balances to simulate changes in lake isotopic signature and water quality. Results highlight that lake water evolution depends mainly on the location and the intensity of recharge changes. Lake water isotopic composition appears to be particularly sensitive to future changes in recharge for lakes with between 50 % and 80 % of groundwater in their total inflows.